(1) Thereflectivity distributionat2

(1) Thereflectivity distributionat2.5kmheightshowsthegen-
eration oftheorganizedcloudsystem.Thereisastrongtem-
poral variationintheverticalstructureofradarreflectivity with
local maximumduringthelatemorningandafternoonhours.
Relativelyshallowecho-topheightsareobservedduringthelate
night tillearlymorninghours.Itisfoundthatthecloudsare
generallyshallowwithradarechotopslessthan5kmexceptin
the afternoonhourswhenthecloudsgrowdeepertill8–9 km
with significant radarreflectivity values.Theobservationsof
shallow cloudsareconsistentwithearlierreportedresultsby
severalstudies(Sarker,1966, Konwaretal.,2012a, Konwaretal.,
2014). Thetemporalandstructuralevolutionsofthemonsoon
clouds ontheleeward(easternside)sideoftheWGare
reportedhereforthe first time.Thisemphasizestheimportance
of continuousobservationsofthecloudsbyremotesensing
techniqueselsewhere.

ผลลัพธ์ (ไทย) 1:

(1) distributionat2.5kmheightshowsthegen Thereflectivity-eration oftheorganizedcloudsystem Thereisastrongtem-variationintheverticalstructureofradarreflectivity poral ด้วยmaximumduringthelatemorningandafternoonhours ท้องถิ่นRelativelyshallowecho-topheightsareobservedduringthelateคืน tillearlymorninghours Itisfoundthatthecloudsaregenerallyshallowwithradarechotopslessthan5kmexceptinkm afternoonhourswhenthecloudsgrowdeepertill8-9มีค่า radarreflectivity อย่างมีนัยสำคัญ Theobservationsofcloudsareconsistentwithearlierreportedresultsby ตื้นseveralstudies (Sarker, 1966, Konwaretal, 2012a, Konwaretal.,2014) . Thetemporalandstructuralevolutionsofthemonsoonเมฆ (easternside) ontheleeward sideoftheWGarereportedhereforthe ครั้งแรก Thisemphasizestheimportanceของ continuousobservationsofthecloudsbyremotesensingtechniqueselsewhere

ผลลัพธ์ (ไทย) 2:

(1) Thereflectivity distributionat2.5kmheightshowsthegen-
eration oftheorganizedcloudsystem.Thereisastrongtem-
poral variationintheverticalstructureofradarreflectivity
กับท้องถิ่น afternoonhourswhenthecloudsgrowdeepertill8-9 กม. อย่างมีนัยสำคัญ radarreflectivity values.Theobservationsof ตื้น cloudsareconsistentwithearlierreportedresultsby severalstudies (Sarker 1966 Konwaretal., 2012a, Konwaretal., 2014) Thetemporalandstructuralevolutionsofthemonsoon เมฆ ontheleeward (easternside) sideoftheWGare reportedhereforthe แรก time.Thisemphasizestheimportance ของ continuousobservationsofthecloudsbyremotesensing techniqueselsewhere

ผลลัพธ์ (ไทย) 3:

( 1 ) thereflectivity distributionat2.5kmheightshowsthegen -
eration oftheorganizedcloudsystem . thereisastrongtem -

poral variationintheverticalstructureofradarreflectivity กับท้องถิ่น maximumduringthelatemorningandafternoonhours .

relativelyshallowecho topheightsareobservedduringthelate คืน tillearlymorninghours itisfoundthatthecloudsare generallyshallowwithradarechotopslessthan5kmexceptin

.การ afternoonhourswhenthecloudsgrowdeepertill8 – 9 km
ด้วยค่า radarreflectivity อย่างมีนัยสำคัญ theobservationsof

severalstudies ตื้น cloudsareconsistentwithearlierreportedresultsby ( Sarker 1966 konwaretal 2012a konwaretal . , , . ,
2014 ) thetemporalandstructuralevolutionsofthemonsoon
เมฆ ontheleeward ( easternside ) ครั้งแรก sideofthewgare thisemphasizestheimportance

reportedhereforthe .ของ continuousobservationsofthecloudsbyremotesensing
techniqueselsewhere .